supported by the National Key Research and Development Program of China(2023YFF0805800);Strategic Priority Research Program of Chinese Academy of Sciences(Nos.XDB31000000 and XDA19050103);the National Natural Science Foundation of China(No.31900190).
The formation of the Qinghai-Tibet Plateau has long been debated,despite the various proxies used to estimate its paleoelevation.Here,we introduce a novel method to calibrate paleoelevation by comparing the fossil and...
supported by the National Natural Science Foundation of China Basic Science Center for Tibetan Plateau Earth System(41988101);the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0708);the Strategic Priority Research Program of the Chinese Academy of Sciences(XDA20070301);the National Natural Science Foundation of China-Natural Environment Research Council of the United Kingdom Joint Research Program(41661134049 and NE/P013805/1);the National Natural Science Foundation of China(41941016)。
The uplift of eastern Tibet,Asian monsoon development and the evolution of globally significant Asian biodiversity are all linked,but in obscure ways.Sedimentology,geochronology,clumped isotope thermometry,and fossil ...
supported by the Chinese Academy of Sciences(Grant Nos.QYZDY-SSW-DQC001,132B61KYSB20170005,ZDBS-LY-DQC033);the National Natural Science Foundation of China(Grant No.41420104008)。
Numerous field studies have shown that leaf wax n-alkane δD values(δD_(n-alkane))can be used as a proxy for paleoelevation reconstruction.However,the lack of systematic global analysis of δD_(n-alkane) values with ...
supported by the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(2019QZKK0901);the Natural Science Foundation of China(41672211);the China Geological Survey(DD20190059);the Fundamental Research Funds for institute of geology,CAGS(JYYWF201810).
When and how the Tibetan Plateau formed and maintained its thick crust and high elevation on Earth is continuing debated.Specifically,the coupling relationship between crustal thickening and corresponding paleoelevati...
supported by National Science and Technology Major Project (2011ZX05009-001)
We investigate the growth of the northern Tibetan Plateau and associated climate change by applying oxygen and carbon isotopic compositions in Cenozoic strata in the southwestern Qaidam basin. The X-ray diffraction an...
financially supported by the National Natural Science Foundation of China (Grant Nos. 41472207 & 41490615);the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (Grant No. XDB03010401)
The surface uplift history of the Tibetan Plateau has provided a key boundary criterion for various geological, climatic,and environmental events since the Cenozoic. The paleoelevation history of the plateau is organi...
supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB03020000;XDB03010000);the National Natural Science Foundation of China(41430102;41490615;and 41472207);the Ministry of Science and Technology of China(2012CB821906)
Over the last two decades, many quantitative paleoaltimetry reconstructions of the Tibetan Plateau have been published, but they are still preliminary and controversial, although several approaches have been combined ...
the Project of the National Natural Science Foudation of China (Grant No.41372114,41340005,41172162,40972083)
We applied the material balance principle of the denudation volume and sedimentary flux to study the denudation-accumulation system between the Longmen Mountains (Mts.) and the foreland basin. The amount of sediment...
supported by the Knowledge Innovation Project of the Chinese Academy of Sciences (Grant No. KZCX2-YW-Q09-03);National Natural Science Foundation for Distinguished Young Scholar (Grant No. 40625008);National Basic Research Program of China (Grant No. 2009CB421000)
Fossil tooth enamel from herbivores is considered one of the best proxies for paleoclimate and paleoelevation reconstructions, due to its low susceptibility to diagenetic alteration. A synthesis of oxygen and carbon i...
Supported by National Basic Research Program of China (Grant No. 2006CB701401);National Natural Science Foundation of China (Grant Nos. 40802008, 40772012 and 40502005);Research Fund for the Doctoral Program of Higher Education (Grant No. 200807301005);Science and Technology Program of Gansu Province (Grant No. 0806RJYA016)
After detailed studies of leaf area, leaf shape index, petiole length, stomatal density, stomatal index, and carbon isotope discrimination of Ginkgo biloba L., growing in Northwest China, the change trends of these pa...